Titlebook: Climate Change Impacts on Water Resources; Hydraulics, Water Re Ramakar Jha,Vijay P. Singh,Roshni Thendiyath Book 2021 The Editor(s) (if ap

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John Milios,Dimitris P. Sotiropoulosn of surface waters. Land use changes have potentially large impacts on river water quality, e.g., adaptation of cropland to urban area, crop rotations, establishment of new industries, commercial and residential areas etc. Unplanned developments associated with land use change have notably influenc

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John Milios,Dimitris P. Sotiropoulos urban storm drainage network, spillways of major water control structures, etc.). Conventional practice for design of those infrastructures includes determination of magnitude and frequency of extreme precipitation events. The extreme events usually lie in the tail part of the probability distribut

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John Milios,Dimitris P. Sotiropoulos is dynamic in nature. Streamflow is one such component of the hydrologic cycle influenced by a large pool of several influencing hydroclimatic variables in different complex ways. There is a plethora of models for streamflow prediction; however, temporal variation in cause–effect relationship may l

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Deleuze and Guattari’s Smooth Spacesrole in reducing the carrying capacity of channel networks and storage capacity of reservoirs/dams. An important task for most of the hydrologists is to determine the reliable stream flow estimate which causes majority of the sediment transport within river basins/stream channels. The transport effe

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Derrida and the (IM)Possibilities of Justiceers. Over many decades various methodologies have been introduced and applied to the wide range of climatic conditions to predict the water loss from vegetation. Among them FAO-56 Penman-Monteith equation is known to be the widely accepted and it has been validated to the wide range of vegetation an

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Deleuze and Guattari’s Smooth Spaces due to human interventions and change in climate. The change in LULC causes change in evapotranspiration and contributes to further climatic change in the area. Hydrologic extremes occur in a river basin due to the combined effect of climatic extremes and LULC changes. Both climate and LULC change

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